Subduction
material from the Earth's surface is returned to the interior.
earthquake
When one plate slides beneath another it is said to subduct. This is called a subduction zone. However, a continental plate cannot subduct, only an oceanic plate can. When two continental plates collide the land between them is squeezed horizontally, forming mountain ranges. Eventually the continental land masses will fuse together.
Tectonic plates are large pieces of Earth's lithosphere that move and interact with each other. When one tectonic plate slides beneath another in a process called subduction, it can create phenomena like earthquakes and volcanic activity. This process is a key driver of the movement and shaping of Earth's crust.
The process is called subduction. Subduction occurs when one tectonic plate slides beneath another plate due to differences in density, often leading to the formation of deep ocean trenches and volcanic activity.
material from the Earth's surface is returned to the interior.
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Translation.
When one tectonic plate slides under another, a subduction zone is formed. This process creates deep ocean trenches and can lead to the formation of volcanic arcs and earthquakes. The sinking plate eventually melts into the mantle, contributing to the recycling of Earth's crust.
Subduction is the process where one tectonic plate slides beneath another into the Earth's mantle at a convergent plate boundary. This process is responsible for the formation of deep ocean trenches, volcanic arcs, and earthquakes.
The type of boundary where one tectonic plate slides under another is called a convergent boundary. This process is known as subduction, where one plate is forced beneath the other due to differences in density.
Where a tectonic plate slides past another.
collision
They are called slides. They do not have another name.
earthquake
a piston